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活性氮与环保公共政策 被引量:1
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作者 jerry m.melillo Ellis B.Cowling 刘林群 《AMBIO-人类环境杂志》 2002年第2期150-158,共9页
美国和欧洲污染治理政策的一个核心目标,是建立环境中活性氮运移的相关法规和条例。这表现在美国联邦政府的立法上(例如《清洁空气法修正案》和《清洁水法修正案》),以及联合国欧洲经济委员会的各种议定书及其《远程跨边界空气污染公约... 美国和欧洲污染治理政策的一个核心目标,是建立环境中活性氮运移的相关法规和条例。这表现在美国联邦政府的立法上(例如《清洁空气法修正案》和《清洁水法修正案》),以及联合国欧洲经济委员会的各种议定书及其《远程跨边界空气污染公约》上。本文中我们首先回顾一下美国的这两部法规及其实施效果,并将它们与联合国欧洲经济委员会和《远程跨边界空气污染公约》主要在欧洲采用的一些方法进行对比。然后利用密西西比河流域和(或)墨西哥湾氧过少的案例研究结果,重点讨沦运用'系统分析方法'处理区域性活性氮问题的重要性。在列举了与氮治理政策有关的一些无法回答的问题后,我们在文末简要描述了在制定完善的活性氮管理政策过程中将要实施的行动计划。 展开更多
关键词 活性氮 环保公共政策 空气污染 法规
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Adjustment of Forest Ecosystem Root Respiration as Temperature Warms 被引量:8
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作者 Andrew J.Burton jerry m.melillo Serita D.Frey 《Journal of Integrative Plant Biology》 SCIE CAS CSCD 2008年第11期1467-1483,共17页
Adjustment of ecosystem root respiration to warmer climatic conditions can alter the autotrophic portion of soil respiration and influence the amount of carbon available for biomass production. We examined 44 publishe... Adjustment of ecosystem root respiration to warmer climatic conditions can alter the autotrophic portion of soil respiration and influence the amount of carbon available for biomass production. We examined 44 published values of annual forest root respiration and found an increase in ecosystem root respiration with increasing mean annual temperature (MAT), but the rate of this cross-ecosystem increase (Q10 = 1.6) is less than published values for short-term responses of root respiration to temperature within ecosystems (Q10 = 2-3). When specific root respiration rates and root biomass values were examined, there was a clear trend for decreasing root metabolic capacity (respiration rate at a standard temperature) with increasing MAT. There also were tradeoffs between root metabolic capacity and root system biomass, such that there were no instances of high growing season respiration rates and high root biomass occurring together. We also examined specific root respiration rates at three soil warming experiments at Harvard Forest, USA, and found decreases in metabolic capacity for roots from the heated plots. This decline could be due to either physiological acclimation or to the effects of co-occurring drier soils on the measurement date. Regardless of the cause, these findings clearly suggest that modeling efforts that allow root respiration to increase exponentially with temperature, with Q10 values of 2 or more, may over-predict root contributions to ecosystem CO2 efflux for future climates and underestimate the amount of C available for other uses, including net primary productivity. 展开更多
关键词 ACCLIMATION climatic warming root biomass root respiration soil warming.
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